Rapid late-glacial atmospheric CO2 chang
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David J. Beerling; Hilary H. Birks; F. Ian Woodward
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Article
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1995
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John Wiley and Sons
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English
โ 672 KB
The Younger Dryas stadia1 (1 1 000-10000 yr BP) was an abrupt return to a glacial climate during the termination of the last glaciation. We have reconstructed atmospheric CO, concentrations from a high-resolution sequence of fossil Salix herbacea leaves through this climatic oscillation from Kriiken